GEOSCAN Search Results: Fastlink


TitleDetrital zircon geochronology of the western Ellesmerian clastic wedge, northwestern Canada: Insights on Arctic tectonics and the evolution of the northern Cordilleran miogeocline
AuthorBeranek, L P; Mortensen, J K; Lane, L SORCID logo; Allen, T L; Fraser, T A; Hadlari, TORCID logo; Zantvoort, W G
SourceGeological Society of America Bulletin vol. 122, no. 11/12, 2010 p. 1899-1911,
Alt SeriesEarth Sciences Sector, Contribution Series 20090354
PublisherGeological Society of America
Mediapaper; on-line; digital
File formatpdf
ProvinceNorthwest Territories; Yukon; Nunavut
NTS39; 48; 49; 57; 58; 59; 67; 68; 69; 76; 77; 78; 79; 86; 87; 88; 89; 96; 97; 98; 99; 106; 107; 116; 117; 120; 340; 560
AreaArctic Island
Lat/Long WENS-142.0000 -56.0000 84.0000 64.0000
Subjectsgeochronology; tectonics; radiometric dates; radiometric dating; zircon; zircon dates; plate tectonics; tectonic history; tectonic stages; tectonic evolution; tectonic interpretations; tectonic setting; Ellesmerian clastic wedge; Cordilleran; Cordilleran miogeocline; Imperial Formation; Tuttle Formation; Paleozoic; Mississippian; Devonian; Silurian; Mississippian
Illustrationslocation maps; plots
ProgramGEM: Geo-mapping for Energy and Minerals Yukon Sedimentary Basins
Released2010 08 11
AbstractDetrital zircon provenance investigations of mid-Paleozoic sandstone from the western Ellesmerian clastic wedge and Cordilleran miogeocline in northern Yukon and Northwest Territories, northwestern Canada, provide critical new data on the source of foreland basin sedimentation attributed to terrane accretion and plate convergence along the ancestral Arctic margin of North America. Late Devonian and early Mississippian clastic wedge strata yield "exotic" ca. 360 - 390, 430 - 460, 530 - 680, and 1500 - 1600 Ma detrital zircon populations that are consistent with source rocks that originated near the Caledonian and Timanian orogenic belts. Specifically, the Pearya and Arctic Alaska - Chukotka terranes, the landmass of Crockerland, and Caledonian rocks in eastern Greenland are the inferred sources for exotic detrital zircons in clastic wedge strata. Progressive recycling of Ellesmerian foreland basin sediments into the continental margin environment along northwestern Laurentia is indicated by the presence of ca. 360 - 430 Ma and 1500 - 1600 Ma detrital zircons in post-tectonic, middle to late Mississippian miogeoclinal strata in Yukon. Provenance data from these Mississippian samples record a dramatic shift in the source of the Cordilleran miogeocline, since Caledonian and Baltican (Timanide) detrital zircon signatures are not recognized in pre - Late Devonian sedimentary rocks in western Canada. Devonian strata of the Alexander terrane and Yreka subterrane (eastern Klamath terrane) have Caledonian and Baltican detrital zircon age signatures similar to Ellesmerian clastic wedge sandstones, implying that several Cordilleran terranes originated in the paleo-Arctic realm. Speculative correlations suggest that the Arctic Alaska - Chukotka terrane was located to the west of Crockerland and the Canadian Arctic Islands in pre-Cretaceous time, prior to opening of the Amerasian basin. Rifting models for the western Arctic Ocean featuring counter clockwise rotation of the Arctic Alaska - Chukotka terrane away from the Canadian Arctic Islands may need re-evaluation.

Date modified: